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The Acid Micro-Eroders Destroying Ancient Stone Masterpieces

Microscopic Lichenostigma fungi are slowly erasing human history by secreting concentrated oxalic acid that chemically dissolves ancient limestone monuments from the inside out.

Ancient limestone carvings, monuments, and outdoor heritage sites face a silent biological threat known as biodeterioration. Among the principal culprits are microcolonial fungi belonging to the genus Lichenostigma. These resilient, dark-pigmented fungi thrive on exposed rock surfaces, enduring intense ultraviolet radiation, extreme drought, and severe temperature fluctuations.

Despite their microscopic size, Lichenostigma fungi possess a powerful biochemical weapon: the ability to synthesize and excrete substantial amounts of oxalic acid into their immediate microenvironment. When oxalic acid contacts the calcium carbonate (calcite) structure of limestone, a chemical reaction takes place. The acid dissolves the mineral matrix, leaching calcium ions and forming secondary calcium oxalate crystals, such as whewellite and weddellite.

As these micro-reactions recur over decades, the structural integrity of the stone weakens, causing surface pitting, scaling, and eventual loss of fine artistic detail. Furthermore, the expansion of fungal hyphae within micro-fissures exerts physical pressure, accelerating mechanical breakdown alongside chemical weathering. Conservators worldwide struggle to mitigate Lichenostigma colonization without damaging fragile historical artifacts, prompting advanced research into targeted antimicrobial coatings and non-invasive biocides.

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